Asymmetric warming over coastal California and its impact on the premium wine industry

被引:159
作者
Nemani, RR [1 ]
White, MA
Cayan, DR
Jones, GV
Running, SW
Coughlan, JC
Peterson, DL
机构
[1] Univ Montana, Numer Terradynam Simulat Grp, Missoula, MT 59812 USA
[2] Univ Calif San Diego, Scripps Inst Oceanog, Div Climate Res, La Jolla, CA 92093 USA
[3] US Geol Survey, Div Water Resources, La Jolla, CA 92093 USA
[4] So Oregon Univ, Dept Geog, Ashland, OR 97520 USA
[5] NASA, Ecosyst Sci & Technol Branch, Ames Res Ctr, Moffett Field, CA 94035 USA
关键词
climatic change; asymmetric warming; growing season length; wine industry;
D O I
10.3354/cr019025
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Climatic changes over coastal California from 1951 to 1997 may have benefited the premium wine industry, as seen in higher quality wines and larger grape yields. Observed temperature warming trends were asymmetric, with greatest warming at night and during spring. Warming was associated with large increases in eastern Pacific sea surface temperatures (SST) and amounts of atmospheric water vapor. Although the average annual temperature warming trend was modest (1.13degreesC/47 yr), there was a 20 d reduction in frost occurrence and a 65 d increase in frost-free growing season length. In the Napa and Sonoma valleys, warmer winter and spring temperatures advanced the start of the growing season by 18 to 24 d, and enhanced atmospheric water vapor resulted in a 7% reduction in evaporative demand. Given the strong coupling between Pacific SSTs and the coastal California climate, and because regional-scale SSTs persist for 6 to 12 mo, additional research may allow the possibility of predicting vintage quantity and quality from previous winter conditions.
引用
收藏
页码:25 / 34
页数:10
相关论文
共 37 条
[1]  
CAPRIO M, 1993, COLLECTION ANN REPOR
[2]   THE HYDROLOGICAL CYCLE AND ITS INFLUENCE ON CLIMATE [J].
CHAHINE, MT .
NATURE, 1992, 359 (6394) :373-380
[3]  
Coombe B. G., 1987, Acta Horticulturae, P23
[4]   Clouds, precipitation and temperature range [J].
Dai, A ;
DelGenio, AD ;
Fung, IY .
NATURE, 1997, 386 (6626) :665-666
[5]  
DETTINGER MD, 1995, J CLIMATOL, V8, P607
[6]   Potential effects of differential day-night warming in global climate change on crop production [J].
Dhakhwa, GB ;
Campbell, CL .
CLIMATIC CHANGE, 1998, 40 (3-4) :647-667
[7]   Maximum and minimum temperature trends for the globe [J].
Easterling, DR ;
Horton, B ;
Jones, PD ;
Peterson, TC ;
Karl, TR ;
Parker, DE ;
Salinger, MJ ;
Razuvayev, V ;
Plummer, N ;
Jamason, P ;
Folland, CK .
SCIENCE, 1997, 277 (5324) :364-367
[8]  
EBBESMEYER CC, 1990, P 7 ANN PAC CLIM PAC, P115
[9]  
Gaffen DJ, 1999, J CLIMATE, V12, P811, DOI 10.1175/1520-0442(1999)012<0811:CATOUS>2.0.CO
[10]  
2